FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2150023934> ?p ?o ?g. }

• W2150023934 endingPage "163" @default.
• W2150023934 startingPage "148" @default.
• W2150023934 abstract "The preservational condition of benthic foraminifera from tropical intertidal sediments in Cleveland Bay, north Queensland, Australia was examined in order to provide systematic descriptions of taphonomic signatures and semi-quantitative estimates of test degradation. The primary aim was to improve understanding of the processes of test degradation experienced by intertidal foraminifera during early burial. Eight common tropical, intertidal foraminiferal species were examined: Arenoparrella mexicana, Miliammina fusca, Miliammina obliqua and Trochammina inflata from two upper mangrove stations, and Ammonia aoteana, Elphidium excavatum clavatum, Pararotalia venusta and Parrellina hispidula from two mudflat stations. Taphonomic alteration was broadly divided into surface/textural features and larger-scale, structural losses to tests. Surface alteration of calcareous tests was dominated by the etching and roughening associated with dissolution processes, with limited evidence for bioerosion and abrasion. Both surficial etching and larger-scale structural damage were closely related to test architecture, with degradation most intense on porous chamber walls, as opposed to non-porous-areas, interlocular walls and chamber tips. Furthermore, all calcareous species exhibited consistent pathways of degradation whereby the most recently formed chambers were the most vulnerable to degradation. The correspondence between larger-scale test loss and these patterns of surface textural alteration, suggests calcareous test degradation is primarily driven by dissolution. Degradation of agglutinated tests contrasts in a number of ways. Pristine tests of all four species examined exhibited a smooth, outer organic coating, which may be missing from other specimens. The extent to which this initial loss effects further test breakdown is uncertain, but appears to differ between species. M. obliqua and some specimens of A. mexicana exhibited structural damage which corresponded to clear cement losses and agglutinant disaggregation. More generally, agglutinated species displayed fracturing and test breakages which bore no conspicuous relation to cement loss. Furthermore, neither surface alteration nor structural loss affected any part of agglutinated tests preferentially, and therefore pathways of degradation were inconsistent across specimens. The fact that agglutinated tests degrade in a more arbitrary manner, compared with calcareous tests, is taken as evidence that their degradation is (1) not entirely controlled by test architecture, and (2) at least partially driven by physical/mechanical processes. We suggest that, if agglutinated tests are not already inherently weaker than their calcareous counterparts, the loss of organic cements may sufficiently weaken agglutinated tests so as to increase susceptibility to physical damage. Tests were also graded according to the extent to which they were structurally degraded. Average taphonomic grades and taphonomic variability (i.e. standard deviation) for all species at Cocoa Creek were statistically invariant with depth, contrary to expectations based on the concept of progressive burial through a taphonomically-active zone. This indicates that shallow sub-surface sediments are significantly homogenised, and that sediment mixing and infaunal test production imparts a considerable effect on the development of surface and sub-surface dead assemblages at the study site." @default.
• W2150023934 created "2016-06-24" @default.
• W2150023934 creator A5055531791 @default.
• W2150023934 creator A5071751843 @default.
• W2150023934 creator A5088328688 @default.
• W2150023934 date "2009-12-01" @default.
• W2150023934 modified "2023-09-24" @default.
• W2150023934 title "Taphonomic signatures and patterns of test degradation on tropical, intertidal benthic foraminifera" @default.
• W2150023934 cites W1810485278 @default.
• W2150023934 cites W1878137325 @default.
• W2150023934 cites W1967203419 @default.
• W2150023934 cites W1968674021 @default.
• W2150023934 cites W1969535275 @default.
• W2150023934 cites W1973074976 @default.
• W2150023934 cites W1974521733 @default.
• W2150023934 cites W1975497464 @default.
• W2150023934 cites W1977661041 @default.
• W2150023934 cites W1978862266 @default.
• W2150023934 cites W1985282541 @default.
• W2150023934 cites W1990477265 @default.
• W2150023934 cites W1995110175 @default.
• W2150023934 cites W1996097130 @default.
• W2150023934 cites W2000730521 @default.
• W2150023934 cites W2004239806 @default.
• W2150023934 cites W2005572663 @default.
• W2150023934 cites W2005771516 @default.
• W2150023934 cites W2008586401 @default.
• W2150023934 cites W2016299853 @default.
• W2150023934 cites W2016762975 @default.
• W2150023934 cites W2016864795 @default.
• W2150023934 cites W2019865341 @default.
• W2150023934 cites W2025301696 @default.
• W2150023934 cites W2029620213 @default.
• W2150023934 cites W2031605138 @default.
• W2150023934 cites W2032254619 @default.
• W2150023934 cites W2033597923 @default.
• W2150023934 cites W2041117349 @default.
• W2150023934 cites W2042554483 @default.
• W2150023934 cites W2054014497 @default.
• W2150023934 cites W2056692175 @default.
• W2150023934 cites W2057707895 @default.
• W2150023934 cites W2060583811 @default.
• W2150023934 cites W2061187609 @default.
• W2150023934 cites W2062625406 @default.
• W2150023934 cites W2066316562 @default.
• W2150023934 cites W2069982566 @default.
• W2150023934 cites W2072189619 @default.
• W2150023934 cites W2096549615 @default.
• W2150023934 cites W2096886954 @default.
• W2150023934 cites W2101549778 @default.
• W2150023934 cites W2106029620 @default.
• W2150023934 cites W2111005906 @default.
• W2150023934 cites W2111895884 @default.
• W2150023934 cites W2117133909 @default.
• W2150023934 cites W2125996311 @default.
• W2150023934 cites W2127588065 @default.
• W2150023934 cites W2134548470 @default.
• W2150023934 cites W2136654826 @default.
• W2150023934 cites W2136979125 @default.
• W2150023934 cites W2144545002 @default.
• W2150023934 cites W2147933725 @default.
• W2150023934 cites W2155327856 @default.
• W2150023934 cites W2167650831 @default.
• W2150023934 cites W2169760290 @default.
• W2150023934 cites W2180517354 @default.
• W2150023934 cites W2303283138 @default.
• W2150023934 cites W2313989265 @default.
• W2150023934 cites W2314022116 @default.
• W2150023934 cites W2328166471 @default.
• W2150023934 cites W2329641272 @default.
• W2150023934 cites W2330034430 @default.
• W2150023934 cites W2334607093 @default.
• W2150023934 cites W2489898519 @default.
• W2150023934 cites W2614756240 @default.
• W2150023934 doi "https://doi.org/10.1016/j.marmicro.2009.08.002" @default.
• W2150023934 hasPublicationYear "2009" @default.
• W2150023934 type Work @default.
• W2150023934 sameAs 2150023934 @default.
• W2150023934 citedByCount "41" @default.
• W2150023934 countsByYear W21500239342012 @default.
• W2150023934 countsByYear W21500239342013 @default.
• W2150023934 countsByYear W21500239342014 @default.
• W2150023934 countsByYear W21500239342015 @default.
• W2150023934 countsByYear W21500239342016 @default.
• W2150023934 countsByYear W21500239342017 @default.
• W2150023934 countsByYear W21500239342018 @default.
• W2150023934 countsByYear W21500239342019 @default.
• W2150023934 countsByYear W21500239342021 @default.
• W2150023934 countsByYear W21500239342022 @default.
• W2150023934 countsByYear W21500239342023 @default.
• W2150023934 crossrefType "journal-article" @default.
• W2150023934 hasAuthorship W2150023934A5055531791 @default.
• W2150023934 hasAuthorship W2150023934A5071751843 @default.
• W2150023934 hasAuthorship W2150023934A5088328688 @default.
• W2150023934 hasConcept C10277891 @default.
• W2150023934 hasConcept C111368507 @default.
• W2150023934 hasConcept C123552892 @default.
• W2150023934 hasConcept C127313418 @default.

• next